1-C Coastal Landscapes Flashcards
What are the characteristics of constructive waves?
The swash is stronger than backwash, so they build beaches. This is because the wave loses energy from the friction with the sand, and some water soaks into sand.
They are found in sheltered bays and spits, and are more common in summer.
What are the characteristics of destructive waves?
The backwash is greater than the swash, so they comb beach material back into the sea.
The force from breaking destructive waves is sufficient enough to erode headlands. They are found in exposed bays. They are more common in winter.
Describe the three processes of weathering
- Mechanical - breakdown of rock without changing its chemical composition (e.g. salt weathering - salt crystals form inside the rock and expands and puts pressure on the rock)
- Chemical - breakdown of rock by changing its chemical composition (e.g. carbonating weathering - carbonic acid in rain and seawater react with rocks that contain calcium carbonate and dissolve them)
- Biological - breakdown of rocks by living things (e.g. plant roots break down rocks by growing into cracks on their surface and pushing them apart)
What is mass movement and what are the three types of it?
Mass movement is the shifting of rocks and loose material down a slope. It causes coasts to retreat rapidly. If the material is full of water, it is more likely as it acts as a lubricant and makes the material heavier.
Three Types:
- Slides - material shifts in a straight line
- Slumps - material shifts with a rotation
- Rockfalls - material breaks up and falls down slope
Describe the four process of erosion
- Hydraulic power - waves crash against rock and compress air in the cracks. This puts pressure on the rock and bits break off.
- Abrasion - eroded particles in the water scrape and rub against rock, removing small pieces
- Attrition - eroded particles in the water smash into each other and break into smaller fragments. They become rounded eventually.
- Solution - dissolved carbon dioxide makes sea water acidic. The acid reacts with some rocks, which dissolves them.
Describe the process of transportation of sediment on a coastal landscape
Longshore Drift
- Waves follow the prevailing winds (eastwards)
- The swash carries material up the beach in the same direction as the waves
- The backwash then carries materials down perpendicular to the beach
- Overtime, materials zigzags along the coast
Describe the process of deposition
Deposition - when material carried by the seawater is dropped on the coast.
It occurs when the water does not have enough energy to carry the sediment. Therefore, low energy waves build up beaches - constructive waves.
How does the geological structure of a coastline influence the formation of erosional landforms?
Discordant Coastline - alternating bands of hard and soft rock that are right angles to the coast. They form bays and headlands as the rocks erode at different rates
Concordant coastline - alternating bands of hard and soft rock that are parallel to the coast. Not many erosional landforms are made here
Rocks with lots of joints and faults erode faster.
How are headlands and bays formed?
Formed on discordant coastlines -
- Less resistant rocks are eroded quickly, which forms the bay (gentle slope)
- More resistant rocks are eroded slowly, which forms the headland (steep slope)
How are cliffs and wave cut platforms formed?
- Waves erode mostly at the foot of a cliff. This forms a wave-cut notch, which is enlarged as erosion continues.
- As the rock above the notch becomes unstable, it eventually collapses. The collapsed material is washed away and a new wave-cut notch is created.
- Repeated collapsing results in cliffs retreating.
- A wave-cut platform is the platform that is left bending as the cliff retreats
How are caves formed?
Headlands often have cracks in them.
Through waves repeatedly crashing into them, mostly by abrasion and hydraulic power, the crack is enlarged and a wave forms.
How are arches formed?
When the waves continue to erode the cave, it eventually deepens and breaks through. This is called an arch (e.g. Durdle Door in Dorset)
How are stacks formed?
Erosion continues to wear away the rock, which supports the arch, until it eventually collapses. This forms a stack - an isolated rock that is separate from the headland (e.g. Old Harry in Dorset)
How are beaches formed by deposition?
Beaches are found between the high water mark and the low water mark. They are formed by constructive waves depositing shingle and sand.
How are spits formed by deposition?
- Spits form at sharp bends in the coastline
- Longshore drift transports sand and shingle past the bend and deposits it into the sea.
- Strong winds and waves can curve the end (forming a recurved end)
- The sheltered area behind the spit is protected from waves - plants accumulate here (it can become a mud flat or a salt marsh)